Using a gridded global dataset to characterize regional hydroclimate in central Chile
Using a gridded global dataset to characterize regional hydroclimate in central Chile
Central Chile is facing dramatic projections of climate change, with a consensus for declining precipitation, negatively affecting hydropower generation and irrigated agriculture. Rising from sea level to 6000 m within a distance of 200 km, precipitation characterization is difficult because of a lack of long-term observations, especially at higher elevations. For understanding current mean and extreme conditions and recent hydroclimatological change, as well as to provide a baseline for downscaling climate model projections, a temporally and spatially complete dataset of daily meteorology is essential. The authors use a gridded global daily meteorological dataset at 0.25° resolution for the period 1948-2008, adjusted by monthly precipitation observations interpolated to the same grid using a cokriging method with elevation as a covariate. For validation, daily statistics of the adjusted gridded precipitation are compared to station observations. For further validation, a hydrology model is driven with the gridded 0.25° meteorology and streamflow statistics are compared with observed flow. The high elevation precipitation is validated by comparing the simulated snow extent to Moderate Resolution Imaging Spectroradiometer (MODIS) images. Results show that the daily meteorology with the adjusted precipitation can accurately capture the statistical properties of extreme events as well as the sequence of wet and dry events, with hydrological model results displaying reasonable agreement with observed streamflow and snow extent. This demonstrates the successful use of a global gridded data product in a relatively data-sparse region to capture hydroclimatological characteristics and extremes.
Agriculture, Anthropogenic effects, Climate prediction, Flood events, Hydrologic models
251-265
Demaria, E. M.C.
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Maurer, E. P.
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Sheffield, J.
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Bustos, E.
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Poblete, D.
09c18553-21c4-47c8-9285-496d4f3eb666
Vicuña, S.
7e7a3777-78f9-46b2-b0e9-c7c892f0e3dc
Meza, F.
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February 2013
Demaria, E. M.C.
344329d2-e57c-45ce-8b07-7d6bb044f349
Maurer, E. P.
0e34ce05-e351-4c20-bf76-9916e5c47f91
Sheffield, J.
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Bustos, E.
8d087812-3566-436c-a8a3-0eb6949df6f5
Poblete, D.
09c18553-21c4-47c8-9285-496d4f3eb666
Vicuña, S.
7e7a3777-78f9-46b2-b0e9-c7c892f0e3dc
Meza, F.
522232b3-5027-4809-bb37-e51bfb3a5d82
Demaria, E. M.C., Maurer, E. P., Sheffield, J., Bustos, E., Poblete, D., Vicuña, S. and Meza, F.
(2013)
Using a gridded global dataset to characterize regional hydroclimate in central Chile.
Journal of Hydrometeorology, 14 (1), .
(doi:10.1175/JHM-D-12-047.1).
Abstract
Central Chile is facing dramatic projections of climate change, with a consensus for declining precipitation, negatively affecting hydropower generation and irrigated agriculture. Rising from sea level to 6000 m within a distance of 200 km, precipitation characterization is difficult because of a lack of long-term observations, especially at higher elevations. For understanding current mean and extreme conditions and recent hydroclimatological change, as well as to provide a baseline for downscaling climate model projections, a temporally and spatially complete dataset of daily meteorology is essential. The authors use a gridded global daily meteorological dataset at 0.25° resolution for the period 1948-2008, adjusted by monthly precipitation observations interpolated to the same grid using a cokriging method with elevation as a covariate. For validation, daily statistics of the adjusted gridded precipitation are compared to station observations. For further validation, a hydrology model is driven with the gridded 0.25° meteorology and streamflow statistics are compared with observed flow. The high elevation precipitation is validated by comparing the simulated snow extent to Moderate Resolution Imaging Spectroradiometer (MODIS) images. Results show that the daily meteorology with the adjusted precipitation can accurately capture the statistical properties of extreme events as well as the sequence of wet and dry events, with hydrological model results displaying reasonable agreement with observed streamflow and snow extent. This demonstrates the successful use of a global gridded data product in a relatively data-sparse region to capture hydroclimatological characteristics and extremes.
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Published date: February 2013
Keywords:
Agriculture, Anthropogenic effects, Climate prediction, Flood events, Hydrologic models
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Local EPrints ID: 480771
URI: http://eprints.soton.ac.uk/id/eprint/480771
ISSN: 1525-755X
PURE UUID: 2b09e42b-ec02-4dab-a42c-dad482d975ee
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Date deposited: 09 Aug 2023 17:11
Last modified: 17 Mar 2024 03:40
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Contributors
Author:
E. M.C. Demaria
Author:
E. P. Maurer
Author:
E. Bustos
Author:
D. Poblete
Author:
S. Vicuña
Author:
F. Meza
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